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One of the most important characteristics of systems of stratification is their degree of flexibility.In an open system of stratification:
Low-viscosity Lavas
Lava flows that are thin, runny, and able to travel long distances due to their low resistance to flow.
Volatile-rich Eruptions
Volatile-rich eruptions refer to volcanic eruptions that expel a high amount of volatile compounds, such as water vapor and gases, leading to explosive phenomena.
High-viscosity
Describes a fluid that is thick and resistant to flow, often characteristic of some types of lava.
Lava Tube
A long, tubular opening under the crust of solidified lava and representing an active or partially emptied subsurface channel of lava.
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